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- W2325386419 abstract "近年我国で発生した強地震の鉛直アレー実測記録を用いて、表層地盤中での地震波動のエネルギーの流れをSH波重複反射理論に基づき計算した。その結果、波動エネルギーは基盤から地表に向かうほど低減する一般的傾向が見られた。これはインピーダンスが大きく異なる層境界で下方に戻されるためで、多くの地点で深度100m程度での上昇波エネルギーのうち３割以下しか地表まで到達しない。さらに、地盤中で失われる内部損失エネルギーと上昇エネルギーの割合は地盤各層の減衰定数と良い相関があることが分かった。また、深度100m程度での水平動の入射エネルギーはマグニチュードと震源距離によるごく単純な計算式により概略評価できることが分かった。" @default.
- W2325386419 created "2016-06-24" @default.
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- W2325386419 date "2011-01-01" @default.
- W2325386419 modified "2023-10-03" @default.
- W2325386419 title "Subsurface Energy Flow of Seismic Wave based on Strong Motion Records Observed in Vertical Arrays" @default.
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- W2325386419 doi "https://doi.org/10.5610/jaee.11.1_14" @default.
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